PlaceDossier / BC places / Aquifers
BC aquifer 1197 · sand and gravel · 131 km² · Fraser Valley
Aquifer 1197: Greendale Deep
Aquifer 1197 (Greendale Deep) is a confined sand and gravel (glacio-marine) aquifer of 131 km² in the Fraser Valley regional district, mapped in 2019. The province rates its productivity not rated, its vulnerability to contamination from the surface low, and the demand on it not rated. 14 wells on record are linked to it; water-supply wells there are typically 71.7 m deep and tested at a median 379 L/min.
How the province rates it
Productivity not rated, vulnerability low, demand not rated.
| Rating | What it means | |
|---|---|---|
| Productivity how much water the aquifer gives up to wells, judged from well yields, the aquifer material and pumping tests | not rated | The province hasn't rated this for this aquifer. |
| Vulnerability how easily something spilled at the ground surface could reach the water, judged from what lies above the aquifer and how deep the water is | low (class C) | Better protected (class C), usually by clay or silt above it or deep water. Not immune: a gap in the cover or a badly sealed well can still let contaminants in. |
| Demand how much the aquifer is used now, judged from the number and density of wells and what they're used for | not rated | The province hasn't rated this for this aquifer. |
| Level of development Inferred demand compared with productivity | unclear | Unclear: the province hasn't rated both demand and productivity. |
Ratings are the province's, set when the aquifer was mapped (2019) from wells, geology and local studies. Vulnerability is about the ground, not what's built on it: a well-protected aquifer under a busy area can still be at more risk than an exposed one in the bush.
Sources: Ground Water Aquifers, Water Protection and Sustainability Branch, Province of BC and Groundwater Wells (GWELLS), Province of BC, as published on October 1, 2026 (Open Government Licence – British Columbia); ratings explained after Berardinucci and Ronneseth (2002), Guide to Using the BC Aquifer Classification Maps for the Protection and Management of Groundwater, BC Ministry of Water, Land and Air Protection. Summaries by PlaceDossier.
The wells in it
14 wells on record are linked to this aquifer.
| Wells linked | 14 (10 water-supply) |
|---|---|
| Water-supply well depth | median 71.7 m; middle half 60.4 m to 74.3 m (10 wells) |
| Tested yield | median 379 L/min; middle half 303 L/min to 946 L/min (9 wells tested) |
| Water level below ground | median 3 m when drilled (9 wells) |
| Drilled | 1955 to 2016 |
This aquifer's medianIts middle half of wellsAnother BC aquifer's median
Depths are how deep the driller finished the well; yields are the driller's test, often an hour or less, in litres per minute. A domestic well's yield is usually judged against the household's peak use; ask a driller what's enough for yours.
Where it is
Outline simplified by us from the provincial map; not for locating a lot. It lies under Chilliwack (85%), Abbotsford (13%).
| Kind | Confined sand and gravel - glacio-marine |
|---|---|
| Geological unit | Pleistocene, Late Wisconsin Glaciomarine Outwash |
| Location, as described | Chilliwack – Fraser Lowland |
| Area | 131 km² |
| Mapped | 2019 |
Confined: a layer of clay, silt or till lies over it, which slows water (and spills) from the surface; wells reach it through that layer. The province's page for this aquifer lists the studies behind it and its observation wells: GWELLS aquifer 1197.
Sources: Ground Water Aquifers, Water Protection and Sustainability Branch, Province of BC and Groundwater Wells (GWELLS), Province of BC, as published on October 1, 2026 (Open Government Licence – British Columbia); ratings explained after Berardinucci and Ronneseth (2002), Guide to Using the BC Aquifer Classification Maps for the Protection and Management of Groundwater, BC Ministry of Water, Land and Air Protection. Summaries by PlaceDossier.
What this record doesn't cover
The province maps aquifers where wells and studies give enough to go on, mostly in settled valleys; most of BC isn't mapped, and a lot outside every outline can still have groundwater. Outlines are drawn from geology and well logs at the scale of the study, so an edge can be well off on the ground, and one aquifer can lie under another. Wells are linked to an aquifer by provincial staff from the driller's log: not every well inside an outline is linked, and well depths and yields are as the driller reported them, often from a short test.
These are mapped ratings and drillers' records, not a test of any one lot. Before you buy a property on a well, or plan to drill, ask a qualified hydrogeologist or a registered well driller what this aquifer gives where you are, and test the water.